3,838 research outputs found

    Lagrangian-Eulerian Methods for Uniqueness in Hydrodynamic Systems

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    We present a Lagrangian-Eulerian strategy for proving uniqueness and local existence of solutions in path spaces of limited smoothness for a class of incompressible hydrodynamic models including Oldroyd-B type complex fluid models and zero magnetic resistivity magneto-hydrodynamics equations

    Energy Spectrum of Quasi-Geostrophic Turbulence

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    We consider the energy spectrum of a quasi-geostrophic model of forced, rotating turbulent flow. We provide a rigorous a priori bound E(k) <= Ck^{-2} valid for wave numbers that are smaller than a wave number associated to the forcing injection scale. This upper bound separates this spectrum from the Kolmogorov-Kraichnan k^{-{5/3}} energy spectrum that is expected in a two-dimensional Navier-Stokes inverse cascade. Our bound provides theoretical support for the k^{-2} spectrum observed in recent experiments

    An incompressible 2D didactic model with singularity and explicit solutions of the 2D Boussinesq equations

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    We give an example of a well posed, finite energy, 2D incompressible active scalar equation with the same scaling as the surface quasi-geostrophic equation and prove that it can produce finite time singularities. In spite of its simplicity, this seems to be the first such example. Further, we construct explicit solutions of the 2D Boussinesq equations whose gradients grow exponentially in time for all time. In addition, we introduce a variant of the 2D Boussinesq equations which is perhaps a more faithful companion of the 3D axisymmetric Euler equations than the usual 2D Boussinesq equations.Comment: 9 pages; simplified a solution formula in section 4 and added a sentence on the time growth rate in the solutio

    Inviscid models generalizing the 2D Euler and the surface quasi-geostrophic equations

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    Any classical solution of the 2D incompressible Euler equation is global in time. However, it remains an outstanding open problem whether classical solutions of the surface quasi-geostrophic (SQG) equation preserve their regularity for all time. This paper studies solutions of a family of active scalar equations in which each component uju_j of the velocity field uu is determined by the scalar θ\theta through uj=RΛ1P(Λ)θu_j =\mathcal{R} \Lambda^{-1} P(\Lambda) \theta where R\mathcal{R} is a Riesz transform and Λ=(Δ)1/2\Lambda=(-\Delta)^{1/2}. The 2D Euler vorticity equation corresponds to the special case P(Λ)=IP(\Lambda)=I while the SQG equation to the case P(Λ)=ΛP(\Lambda) =\Lambda. We develop tools to bound uL\|\nabla u||_{L^\infty} for a general class of operators PP and establish the global regularity for the Loglog-Euler equation for which P(Λ)=(log(I+log(IΔ)))γP(\Lambda)= (\log(I+\log(I-\Delta)))^\gamma with 0γ10\le \gamma\le 1. In addition, a regularity criterion for the model corresponding to P(Λ)=ΛβP(\Lambda)=\Lambda^\beta with 0β10\le \beta\le 1 is also obtained
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